{"id":33949,"date":"1998-01-01T00:00:00","date_gmt":"1998-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/hidroquimica-e-intrusion-marina-en-el-campo-de-dalias-almeria\/"},"modified":"1998-01-01T00:00:00","modified_gmt":"1998-01-01T00:00:00","slug":"hidroquimica-e-intrusion-marina-en-el-campo-de-dalias-almeria","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/hidroquimica-e-intrusion-marina-en-el-campo-de-dalias-almeria\/","title":{"rendered":"Hidroquimica e intrusion marina en el campo de dalias (almeria)."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Luis Molina Sanchez <\/strong><\/h2>\n<p>La presente investigaci\u00f3n se ha centrado en el campo de dal\u00edas (almer\u00eda), teniendo como objetivos fundamentales llegar a conocer mejor el funcionamiento hidrogeol\u00f3gico de las unidades acu\u00edferas y el origen de la salinizaci\u00f3n de las aguas. Adem\u00e1s, he perseguido otra serie de objetivos parciales: definir las \u00e1reas de recarga y descarga del sistema para poner luz a la estructura de circulaci\u00f3n subterr\u00e1nea y a las conexiones entre las diferentes unidades acu\u00edferas, para lo que he utilizado la temperatura como trazado f\u00edsico. Diferenciar las facies hidroqu\u00edmicas existentes para deducir los qu\u00edmicos que tienen lugar entre agua y roca. Deducir el movimiento y el comportamiento del agua dentro del acu\u00edfero. En el campo de dal\u00edas se distinguen tres unidades acu\u00edferas, que son: balerma- las marinas, balanegra y aguadulce. En la unidad de balerma-las marinas, el material acu\u00edfero son las calcarenitas pliocenas, la media de la conductividad electrica es de 3100 ms\/cm y la facies dominante es la clorurada s\u00f3dica. La salinizaci\u00f3n se debe principalmente al lixiviado de los materiales pliocenos.  la unidad de balanegra ocupa la mitad occidental del campo. El material acu\u00edfero es fundamentalmente las calizas y dolom\u00edas de g\u00e1dor. El valor medio de la conductividad es de 1024 ms\/cm. El origen de la salinizaci\u00f3n se debe a los materiales miocenos, a aguas salobres y a la disoluci\u00f3n de los materiales sulfatados.  en balanegra la salinizaci\u00f3n es por intrusi\u00f3n marina. La unidad de aguadulce es la de mayor complejidad y de geometr\u00eda peor conocida. En cortes trasversales se suceden varias formaciones acu\u00edferas separadas por otras tantas formaciones de baja permeabilidad, dando lugar a un acu\u00edfero multicapa. La conductividad media de las aguas es de 3789 ms\/cm. La facies dominante es la cloruda s\u00f3dica. La salinizaci\u00f3n de las aguas es debido a la intrusi\u00f3n marina y a la disoluci\u00f3n de los materiales miocenos y pliocenos. Los<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Hidroquimica e intrusion marina en el campo de dalias (almeria).<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Hidroquimica e intrusion marina en el campo de dalias (almeria). <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Luis Molina Sanchez <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1998<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n<h3>Direcci\u00f3n y tribunal<\/h3>\n<ul>\n<li><strong>Director de la tesis<\/strong>\n<ul>\n<li>Antonio Pulido Bosch<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Jos\u00e9 Luis Mart\u00ednez Vidal <\/li>\n<li>Ignacio Morell Evangelista (vocal)<\/li>\n<li>Luigi Tulipano (vocal)<\/li>\n<li>Antonio Castillo Martin (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Luis Molina Sanchez La presente investigaci\u00f3n se ha centrado en el campo de dal\u00edas (almer\u00eda), teniendo como [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center 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